The prophecy is more than seeing into the future. For the prophecy sees without the element of time. For the prophecy sees things as they were, as they are, and as they always shall be.
Monday, October 31, 2022
Indian Point’s Final Days Before the Sixth Seal (Revelation 6:12)
Seismic Activity Before the Sixth Seal: Revelation 6
Reported seismic-like event (likely no quake): Manhattan, 1.1 mi south of Brooklyn, Kings County, Nueva York, USA, Wednesday, Jul 20, 2022 at 2:54 pm (GMT -4) – 1 day 1 hours ago
Event status: disregarded [?]
Updated: Thu, Jul 21, 2022 19:31 GMT – just now
20 Jul 18:59 UTC: First to report: VolcanoDiscovery after 5 minutes.
Earthquake details
Date & timeJul 20, 2022 18:54:37 UTC – 1 day 1 hours agoLocal timeWednesday, Jul 20, 2022 at 2:54 pm (GMT -4)StatusdisregardedMagnitudeunknown (3?)Depth10.0 kmEpicenter40.63402°N / 73.94743°W (Kings, Nueva York, United States)ShakingWeak shakingFelt1 reportPrimary data sourceVolcanoDiscovery (User-reported shaking)Nearby2 km (1 mi) S of Brooklyn (pop: 2,300,700) | Show on map | Quakes nearby
2 km (1 mi) SSE of Flatbush (pop: 93,400) | Show on map | Quakes nearby
3 km (2 mi) SSW of Rugby (pop: 178,500) | Show on map | Quakes nearby
4 km (3 mi) E of Borough Park (pop: 149,200) | Show on map | Quakes nearby
4 km (3 mi) NNE of Gravesend (pop: 112,200) | Show on map | Quakes nearby
5 km (3 mi) N of Sheepshead Bay(pop: 122,500) | Show on map | Quakes nearby
10 km (6 mi) SSE of New York (pop: 8,175,100) | Show on map | Quakes nearby
327 km (203 mi) NE of Washington (District of Columbia) (pop: 601,700) | Show on map | Quakes nearbyWeather at epicenterClear Sky 34.4°C (94 F), humidity: 48%, wind: 3 m/s (6 kts) from S
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Saturday, October 29, 2022
New York Subways at the Sixth Seal (Revelation 6)
How vulnerable are NYC’s underwater subway tunnels to flooding?
Ashley FettersNew York City is full of peculiar phenomena—rickety fire escapes; 100-year-old subway tunnels; air conditioners propped perilously into window frames—that can strike fear into the heart of even the toughest city denizen. But should they? Every month, writer Ashley Fetters will be exploring—and debunking—these New York-specific fears, letting you know what you should actually worry about, and what anxieties you can simply let slip away.
The 25-minute subway commute from Crown Heights to the Financial District on the 2/3 line is, in my experience, a surprisingly peaceful start to the workday—save for one 3,100-foot stretch between the Clark Street and Wall Street stations, where for three minutes I sit wondering what the probability is that I will soon die a torturous, claustrophobic drowning death right here in this subway car.
The Clark Street Tunnel, opened in 1916, is one of approximately a dozen tunnels that escort MTA passengers from one borough to the next underwater—and just about all of them, with the exception of the 1989 addition of the 63rd Street F train tunnel, were constructed between 1900 and 1936.
Each day, thousands of New Yorkers venture across the East River and back again through these tubes buried deep in the riverbed, some of which are nearing or even past their 100th birthdays. Are they wrong to ponder their own mortality while picturing one of these watery catacombs suddenly springing a leak?
Mostly yes, they are, says Michael Horodniceanu, the former president of MTA Capital Construction and current principal of Urban Advisory Group. First, it’s important to remember that the subway tunnel is built under the riverbed, not just in the river—so what immediately surrounds the tunnel isn’t water but some 25 feet of soil. “There’s a lot of dirt on top of it,” Horodniceanu says. “It’s well into the bed of the bottom of the channel.”
And second, as Angus Kress Gillespie, author of Crossing Under the Hudson: The Story of the Holland and Lincoln Tunnels, points out, New York’s underwater subway tunnels are designed to withstand some leaking. And withstand it they do: Pumps placed below the floor of the tunnel, he says, are always running, always diverting water seepage into the sewers. (Horodniceanu says the amount of water these pumps divert into the sewer system each day numbers in the thousands of gallons.)
Additionally, MTA crews routinely repair the grouting and caulking, and often inject a substance into the walls that creates a waterproof membrane outside the tunnel—which keeps water out of the tunnel and relieves any water pressure acting on its walls. New tunnels, Horodniceanu points out, are even built with an outside waterproofing membrane that works like an umbrella: Water goes around it, it falls to the sides, and then it gets channeled into a pumping station and pumped out.
Of course, the classic New York nightmare scenario isn’t just a cute little trickle finding its way in. The anxiety daydream usually involves something sinister, or seismic. The good news, however, is that while an earthquake or explosion would indeed be bad for many reasons, it likely wouldn’t result in the frantic flooding horror scene that plays out in some commuters’ imaginations.
The Montague Tube, which sustained severe damage during Hurricane Sandy.
MTA New York City Transit / Marc A. Hermann
Horodniceanu assures me that tunnels built more recently are “built to withstand a seismic event.” The older tunnels, however—like, um, the Clark Street Tunnel—“were not seismically retrofitted, let me put it that way,” Horodniceanu says. “But the way they were built is in such a way that I do not believe an earthquake would affect them.” They aren’t deep enough in the ground, anyway, he says, to be too intensely affected by a seismic event. (The MTA did not respond to a request for comment.)
One of the only real threats to tunnel infrastructure, Horodniceanu adds, is extreme weather. Hurricane Sandy, for example, caused flooding in the tunnels, which “created problems with the infrastructure.” He continues, “The tunnels have to be rebuilt as a result of saltwater corroding the infrastructure.”
Still, he points out, hurricanes don’t exactly happen with no warning. So while Hurricane Sandy did cause major trauma to the tunnels, train traffic could be stopped with ample time to keep passengers out of harm’s way. In 2012, Governor Andrew Cuomo directed all the MTA’s mass transit services to shut down at 7 p.m. the night before Hurricane Sandy was expected to hit New York City.
And Gillespie, for his part, doubts even an explosion would result in sudden, dangerous flooding. A subway tunnel is not a closed system, he points out; it’s like a pipe that’s open at both ends. “The force of a blast would go forwards and backwards out the exit,” he says.
So the subway-train version of that terrifying Holland Tunnel flood scene in Sylvester Stallone’s Daylight is … unrealistic, right?
“Yeah,” Gillespie laughs. “Yeah. It is.”
Got a weird New York anxiety that you want explored? E-mail tips@curbed.com, and we may include it in a future column.
A Closer Look At The Sixth Seal (Revelation 6:12)
Thursday, October 27, 2022
The History of Earthquakes In New York Before the Sixth Seal (Revelation 6:12)
The History of Earthquakes In New York
Wednesday, October 26, 2022
THE SIXTH SEAL: NEW YORK CITY (REVELATION 6:12)
Earthquake activity in the New York City area
Background
Earthquakes and geologically mapped faults in the Northeastern U.S.
The Ramapo fault and other New York City area faults
The Quakes Preceding the Sixth Seal: Revelation 6:12
East Coast Quakes: What to Know About the Tremors Below
By Meteorologist Dominic Ramunni Nationwide PUBLISHED 7:13 PM ET Aug. 11, 2020 PUBLISHED 7:13 PM EDT Aug. 11, 2020
People across the Carolinas and Mid-Atlantic were shaken, literally, on a Sunday morning as a magnitude 5.1 earthquake struck in North Carolina on August 9, 2020.
Centered in Sparta, NC, the tremor knocked groceries off shelves and left many wondering just when the next big one could strike.
Items lie on the floor of a grocery store after an earthquake on Sunday, August 9, 2020 in North Carolina.
Fault Lines
Compared to the West Coast, there are far fewer fault lines in the East. This is why earthquakes in the East are relatively uncommon and weaker in magnitude.
That said, earthquakes still occur in the East.
According to Spectrum News Meteorologist Matthew East, “Earthquakes have occurred in every eastern U.S. state, and a majority of states have recorded damaging earthquakes. However, they are pretty rare. For instance, the Sparta earthquake Sunday was the strongest in North Carolina in over 100 years.”
While nowhere near to the extent of the West Coast, damaging earthquakes can and do affect much of the eastern half of the country.
For example, across the Tennesse River Valley lies the New Madrid Fault Line. While much smaller in size than those found farther west, the fault has managed to produce several earthquakes over magnitude 7.0 in the last couple hundred years.
In 1886, an estimated magnitude 7.0 struck Charleston, South Carolina along a previously unknown seismic zone. Nearly the entire town had to be rebuilt.
Vulnerabilities
The eastern half of the U.S. has its own set of vulnerabilities from earthquakes.
Seismic waves actually travel farther in the East as opposed to the West Coast. This is because the rocks that make up the East are tens, if not hundreds, of millions of years older than in the West.
These older rocks have had much more time to bond together with other rocks under the tremendous pressure of Earth’s crust. This allows seismic energy to transfer between rocks more efficiently during an earthquake, causing the shaking to be felt much further.
This is why, during the latest quake in North Carolina, impacts were felt not just across the state, but reports of shaking came as far as Atlanta, Georgia, nearly 300 miles away.
Reports of shaking from different earthquakes of similar magnitude.
Quakes in the East can also be more damaging to infrastructure than in the West. This is generally due to the older buildings found east. Architects in the early-to-mid 1900s simply were not accounting for earthquakes in their designs for cities along the East Coast.
When a magnitude 5.8 earthquake struck Virginia in 2011, not only were numerous historical monuments in Washington, D.C. damaged, shaking was reported up and down the East Coast with tremors even reported in Canada.
Unpredictable
There is no way to accurately predict when or where an earthquake may strike.
Some quakes will have a smaller earthquake precede the primary one. This is called a foreshock.
The problem is though, it’s difficult to say whether the foreshock is in fact a foreshock and not the primary earthquake. Only time will tell the difference.
The United State Geological Survey (USGS) is experimenting with early warning detection systems in the West Coast.
While this system cannot predict earthquakes before they occur, they can provide warning up to tens of seconds in advance that shaking is imminent. This could provide just enough time to find a secure location before the tremors begin.
Much like hurricanes, tornadoes, or snowstorms, earthquakes are a natural occuring phenomenon that we can prepare for.
The USGS provides an abundance of resources on how to best stay safe when the earth starts to quake.
Monday, October 24, 2022
USGS Evidence Shows Power of the Sixth Seal (Revelation 6:12)
New Evidence Shows Power of East Coast Earthquakes
Virginia Earthquake Triggered Landslides at Great Distances
Sunday, October 23, 2022
New York Earthquake: City of the Sixth Seal (Revelation 6:12)
New York earthquake: City at risk of ‚dangerous shaking from far away‘
Joshua Nevett
Published 30th April 2018
SOME of New York City’s tallest skyscrapers are at risk of being shaken by seismic waves triggered by powerful earthquakes from miles outside the city, a natural disaster expert has warned.
Researchers believe that a powerful earthquake, magnitude 5 or greater, could cause significant damage to large swathes of NYC, a densely populated area dominated by tall buildings.
A series of large fault lines that run underneath NYC’s five boroughs, Manhattan, Brooklyn, Queens, The Bronx and Staten Island, are capable of triggering large earthquakes.
Some experts have suggested that NYC is susceptible to at least a magnitude 5 earthquake once every 100 years.
The last major earthquake measuring over magnitude 5.0 struck NYC in 1884 – meaning another one of equal size is “overdue” by 34 years, according their prediction model.
Natural disaster researcher Simon Day, of University College London, agrees with the conclusion that NYC may be more at risk from earthquakes than is usually thought.
EARTHQUAKE RISK: New York is susceptible to seismic shaking from far-away tremors
But the idea of NYC being “overdue” for an earthquake is “invalid”, not least because the “very large number of faults” in the city have individually low rates of activity, he said.
The model that predicts strong earthquakes based on timescale and stress build-up on a given fault has been “discredited”, he said.
What scientists should be focusing on, he said, is the threat of large and potentially destructive earthquakes from “much greater distances”.
The dangerous effects of powerful earthquakes from further away should be an “important feature” of any seismic risk assessment of NYC, Dr Day said.
GETTY
THE BIG APPLE: An aerial view of Lower Manhattan at dusk in New York City
USGS
RISK: A seismic hazard map of New York produced by USGS
“New York is susceptible to seismic shaking from earthquakes at much greater distances” Dr Simon Day, natural disaster researcher
This is because the bedrock underneath parts of NYC, including Long Island and Staten Island, cannot effectively absorb the seismic waves produced by earthquakes.
“An important feature of the central and eastern United States is, because the crust there is old and cold, and contains few recent fractures that can absorb seismic waves, the rate of seismic reduction is low.
Central regions of NYC, including Manhattan, are built upon solid granite bedrock; therefore the amplification of seismic waves that can shake buildings is low.
But more peripheral areas, such as Staten Island and Long Island, are formed by weak sediments, meaning seismic hazard in these areas is “very likely to be higher”, Dr Day said.
“Thus, like other cities in the eastern US, New York is susceptible to seismic shaking from earthquakes at much greater distances than is the case for cities on plate boundaries such as Tokyo or San Francisco, where the crustal rocks are more fractured and absorb seismic waves more efficiently over long distances,” Dr Day said.
In the event of a large earthquake, dozens of skyscrapers, including Chrysler Building, the Woolworth Building and 40 Wall Street, could be at risk of shaking.
“The felt shaking in New York from the Virginia earthquake in 2011 is one example,” Dr Day said.
On that occasion, a magnitude 5.8 earthquake centered 340 miles south of New York sent thousands of people running out of swaying office buildings.
USGS
FISSURES: Fault lines in New York City have low rates of activity, Dr Day said
NYC Mayor Michael Bloomberg said the city was “lucky to avoid any major harm” as a result of the quake, whose epicenter was near Louisa, Virginia, about 40 miles from Richmond.
“But an even more impressive one is the felt shaking from the 1811-1812 New Madrid earthquakes in the central Mississippi valley, which was felt in many places across a region, including cities as far apart as Detroit, Washington DC and New Orleans, and in a few places even further afield including,” Dr Day added.
“So, if one was to attempt to do a proper seismic hazard assessment for NYC, one would have to include potential earthquake sources over a wide region, including at least the Appalachian mountains to the southwest and the St Lawrence valley to the north and east.”
Friday, October 21, 2022
Quakes remind us of the Sixth Seal: Revelation 6
EDITORIAL: Quakes remind S.C. of history, potential threat
The Times and Democrat
As 2021 ended and 2022 began, a series of minor earthquakes affected South Carolina’s Midlands.
Elgin, a community of fewer than 2,000 residents near the border of Richland and Kershaw counties, has been the epicenter of the seismic activity, starting with a 3.3-magnitude earthquake on Dec. 27. That quake clattered glass windows and doors in their frames, sounding like a heavy piece of construction equipment or concrete truck rumbling down the road.
In January, more earthquakes have been recorded nearby, ranging from 1.5 to a 2.6 in magnitude. No injury or damage was reported.
Now it’s May – and the quakes are back.
In the early hours of May 9, a 3.3 magnitude earthquake shook the ground in Elgin. The earthquake was followed by two back-to-back earthquakes an hour later registering 1.6 and 1.8 magnitudes.
The three quakes pushed South Carolina’s 2022 earthquake tally to 23, with 19 happening within 35 miles of Columbia. Historically, 70% of earthquakes in the state happen along the Coastal Plain, but because the state isn’t considered a hot spot for earthquake activity, the recent midstate quakes are a bit of a mystery.
According to the South Carolina Emergency Management Division, the state typically averages up to 20 quakes each year. Clusters often happen, like six small earthquakes in just more than a week in 2021 near Jenkinsville, about 38 miles west of the most recent group of tremors.
Though quakes are nothing new to South Carolina, many people in the state are not affected. According to emergency management officials, about 70% of South Carolina earthquakes are located in the Middleton Place-Summerville Seismic Zone, about 12.4 miles (20 kilometers) northwest of Charleston.
Every year South Carolina has a week devoted to earthquake preparedness. And there is good reason for awareness.
Aug. 31, 2021, was the 135th anniversary of the largest earthquake to occur in the eastern U.S. In the late evening on that day in 1886, a magnitude 7 earthquake struck near Charleston, causing the loss of more than 100 lives. Many buildings collapsed or were heavily damaged, with economic losses estimated at more than $100 million in today’s dollars.
The quake was felt throughout much of the eastern and central U.S., with people reporting feeling it as far north as New York and as far west as Illinois and Missouri.
In 1999, retired T&D Publisher Dean B. Livingston wrote about what is recorded locally about that “unscheduled” occurrence that had a lot of people singing “Nearer My God To Thee.”
“The area was pounded for a week by quake shocks from four to 12 times a day. The Times and Democrat wrote of the earth’s rumblings: ‘This earthquake frightened many of the inhabitants into deep religious complex, such as was never known before, bringing about a great religious revival in the churches. …’
“One person wrote that ‘many thought the end of the world had come.’ Some terror-stricken citizens in Rowesville ‘ran to and fro exclaiming: ‘The great Judgment Day is at hand. Lord have mercy on me.” A T&D article noted that ‘many people prayed during the past two weeks who never prayed before.’
“A Sawyerdale citizen reported that ‘the flood of accessions to our various churches is almost unparalleled.’
“Residents of the city of Orangeburg were awakened when the first jolt hit. People in brick homes could hear the bricks ‘grinding together as the forces of the shocks increased.’ Many people complained of a nauseous sensation. Chimneys were shaken down, the Baptist church steeple was damaged and for several nights many families slept in the open, under sheds or in small buildings.
“As late as Oct. 14, The T&D reported that ‘shocks have become so common now that people soon throw off the peculiar feeling that they inspire, and go along as if nothing unusual had occurred. There is no telling when they (shocks) will end. …’
“Over in Vance, the quake was described as a ‘sound, a deep, muffled sound … resembling the distant thunder … the earth was one tremendous oscillation. Buildings creaked … poultry squawked, dogs howled, birds chirped; in fact, everything was completely aroused and powerfully demoralized … from 10 to 11 p.m., nine successive shocks were felt.’
“Two Orangeburg men were fishing on the Edisto River when the first big shock hit. They said the first noise sounded like a loud clap of thunder. ‘This was followed by the usual rumbling which was also very loud and deep. The course of the shake was distinctly marked by the falling of the berries and acorns from the trees as it passed.”
While they have no stories comparable to 1886, people of The T&D Region periodically experience tremors. With a large fault in the earth extending from Charleston into the region, when another major quake will come is unpredictable — but practically certain.
Wednesday, October 19, 2022
Indian Point’s Final Days Before the Sixth Seal (Revelation 6:12)